Articles | Volume 15, issue 8
https://doi.org/10.5194/tc-15-4135-2021
https://doi.org/10.5194/tc-15-4135-2021
Research article
 | 
30 Aug 2021
Research article |  | 30 Aug 2021

Significant mass loss in the accumulation area of the Adamello glacier indicated by the chronology of a 46 m ice core

Daniela Festi, Margit Schwikowski, Valter Maggi, Klaus Oeggl, and Theo Manuel Jenk

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (16 Jun 2021) by Delphine Lannuzel
AR by Daniela Festi on behalf of the Authors (18 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (28 Jun 2021) by Delphine Lannuzel
AR by Daniela Festi on behalf of the Authors (29 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (15 Jul 2021) by Delphine Lannuzel
AR by Daniela Festi on behalf of the Authors (19 Jul 2021)  Author's response   Manuscript 
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Short summary
In our study we dated a 46 m deep ice core retrieved from the Adamello glacier (Central Italian Alps). We obtained a timescale combining the results of radionuclides 210Pb and 137Cs with annual layer counting derived from pollen and refractory black carbon concentrations. Our results indicate that the surface of the glacier is older than the drilling date of 2016 by about 20 years, therefore revealing that the glacier is at high risk of collapsing under current climate warming conditions.